| 摘要: |
| 氮(N)是生物生命活动的基本营养元素，N循环是整个生物圈物质和能量循环的重要组成部分。近几十年来，环境和资源问题的日益突出促进了人们对海洋生态系统的研究及对海洋资源的开发和利用，海洋中的N循环亦受到了广泛关注。尤其是20世纪90年代以来，随着国际地圈与生物圈计划(IGBP)、全球海洋通量联合研究(JGOFS)、全球海洋生态系统动力学研究(GLOBEC)等重大国际合作计划的实施，海洋中的N循环研究取得了重大进展。
本文主要对海洋沉积物中的N循环过程进行了阐述，包括海洋沉积物中N的生物地球化学循环(海洋中N与生物生产过程的关系、早期成岩作用及N的去营养化、沉积物中N循环及其控制机制、颗粒N的形成及其功能、N与其他生源要素循环的关系)及沉积物中N循环的研究方法等，以期对进一步开展N循环的研究有所帮助。 |
| 关键词: 氮循环 生物地球化学循环 海洋沉积物 |
| DOI： |
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| 基金项目:中国科学院海洋研究所调查研究报告第4004号。国家杰出青年科学基金研究资助项目，49925614号。 |
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| NITROGEN CYCLING IN MARINE SEDIMENTS |
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Ma Hongbo, Song Jinming
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Institute of Oceanology, Chinese Academy of Sciences
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| Abstract: |
| This paper reviews nitrogen cycling in marine sediments and consists of three parts：
1. Nitrogen Cycling Processes in Marine Sediments
(1) Nitrogen and primary production
Nitrogen regenerated from marine sediments can contribute largely to primary production. About 30%-80% of nitrogen consumed by phytoplankton is attributed to sediment mineralization and NH4+ (ammonium) is the preferred phase utilized. Benthic heterotrophic bacteria have a large impact on nitrogen cycling and can act as net N consumers sometimes.
(2) Early diagenesis and nutrients loss
Early diagenesis includes oxic and anoxic mineralization. Part of the regenerated NH4+ can be transformed into N2 by the nitrification-denitrification coupling, which leads to nutrient loss from the marine ecosystem. NH4+ adsorption in sediment is another pathway for nutrient loss.
(3) Nitrogen cycling and the controlling factors
NH4+ released from sediments can be assimilated by benthic organisms and diffuse to overlying water or be oxdized into NO3- (nitrate). The role of sediment as a source or sink for nitrogen in seawater is governed by the relative rates of ammonium, nitrate and N2 production. The nitrogen cycling process varies with time and space and the controlling factors includes: temperature, organic matter content, benthic bioturbation. etc.
(4) The formation and function of particulate nitrogen
PN (particulate nitrogen) is mainly formed biogenically. Amino acids account for 30%-60% of the organic nitrogen in particulates. PN can be mineralized or uptaken during sedimentation. The most attractive focus on PN is its function in the marine ecosystem food web.
(5) Nitrogen cycling and other biogenic element cyclings
Nitrogen cycling is in closely correlated with C and P cycling. The efficiency of N and P cycling increases with increased organic carbon loading in sediments. The atomic ratio of C, N, P in sediment deviates from the Redfield ratio of 106: 16: 1 and the former is a very important parameter in nitrogen cycling model construction.
2. Methods for nitrogen cycling research
Research on nitrogen cycling in marine sediments usually focuses on two aspects: nitrogen in sediment and nitrogen in porewater, on which much work has been done on the pore-water. The rates of mineralization, nitrification, denitrification and the exchange fluxes between sediment and overlying water can be measured. Acetylene (C2H2) inhibition technique and 15N tracer technique are most widely used. Analysis for sediment solid is not sufficient, only NH4+ adsorption concentration and total organic nitrogen can be measured.
3. Perspectives on nitrogen cycling research
It has been known that particulate size and organic matter composition in sediments can control nitrogen cycling significantly. So more attention should be paid to these two factors in further research. |
| Key words: nitrogen cycling marine sediments |
